Soil identification and chemometrics for direct determination of nitrate in soils using FTIR-ATR mid-infrared spectroscopy

被引:110
作者
Linker, R [1 ]
Shmulevich, I [1 ]
Kenny, A [1 ]
Shaviv, A [1 ]
机构
[1] Technion Israel Inst Technol, Fac Civil & Environm Engn, Lowdermilk Div Agr Engn, IL-32000 Haifa, Israel
关键词
cross-correlation; neural network; principal component analysis (PCA); soil constituents interference;
D O I
10.1016/j.chemosphere.2005.03.034
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The use of mid-infrared attenuated total reflectance (ATR) spectroscopy enables direct measurement of nitrate concentration in soil pastes, but strong interfering absorbance bands due to water and soil constituents limit the accuracy of straightforward determination. Accurate subtraction of the water spectrum improves the correlation between nitrate concentration and its v(3) vibration band around 1350 cm(-1). However, this correlation is soil-dependent, due mostly to varying contents of carbonate, whose absorbance band overlaps the nitrate band. In the present work, a two-stage method is developed: First, the soil type is identified by comparing the "fingerprint" region of the spectrum (8001200 cm(-1)) to a reference spectral library. In the second stage, nitrate concentration is estimated using the spectrum interval that includes the nitrate band, together with the soil type previously identified. Three methods are compared for estimating nitrate concentration: integration of the nitrate absorbance band, cross-correlation with a reference Spectrum, and principal component analysis (PCA) followed by a neural network. When using simple band integration, the use of soil specific calibration curves leads to determination errors ranging from 5.5 to 24 mg[N]/kg[dry soil] for the mineral soils tested. The cross-correlation technique leads to similar results. The combination of soil identification with PCA and neural network modeling improves the predictions, especially for soils containing calcium carbonate. Typical prediction errors for light non-calcareous soils are about 4 mg[N]/kg[dry soil], whereas for soils containing calcium carbonate they range from 6 to 20 mg[N]/kg[dry soil], which is less than four percent of the concentration range investigated. (C) 2005 Elsevier Ltd. All rights reserved.
引用
收藏
页码:652 / 658
页数:7
相关论文
共 19 条
[1]  
Adsett JF, 1999, APPL ENG AGRIC, V15, P351
[2]  
Birrell SJ, 2000, T ASAE, V43, P197, DOI 10.13031/2013.2694
[3]   ON THE SPECTRAL SUBTRACTION OF WATER FROM THE FT-IR SPECTRA OF AQUEOUS-SOLUTIONS OF PROTEINS [J].
DOUSSEAU, F ;
THERRIEN, M ;
PEZOLET, M .
APPLIED SPECTROSCOPY, 1989, 43 (03) :538-542
[4]  
Ehsani MR, 2001, T ASAE, V44, P1931, DOI 10.13031/2013.6991
[5]   Spectroscopic studies of Pb(II)-sulfate interactions at the goethite-water interface [J].
Elzinga, EJ ;
Peak, D ;
Sparks, DL .
GEOCHIMICA ET COSMOCHIMICA ACTA, 2001, 65 (14) :2219-2230
[6]   Determination of organic matter in soils using radial basis function networks and near infrared spectroscopy [J].
Fidêncio, PH ;
Poppi, RJ ;
de Andrade, JC .
ANALYTICA CHIMICA ACTA, 2002, 453 (01) :125-134
[7]  
Haykin S., 1994, NEURAL NETWORKS COMP, V5, P363, DOI [10.1142/S0129065794000372, DOI 10.1142/S0129065794000372]
[8]  
JOHNSTON CT, 1996, METHODS SOIL ANAL 3
[9]  
Jolliffe I. T., 1986, Principal Component Analysis, DOI [DOI 10.1016/0169-7439(87)80084-9, 10.1007/0-387-22440-8_13, DOI 10.1007/0-387-22440-8_13]
[10]   SPECTRA OF WATER IN THE NEARINFRARED AND MIDINFRARED REGION [J].
LIBNAU, FO ;
KVALHEIM, OM ;
CHRISTY, AA ;
TOFT, J .
VIBRATIONAL SPECTROSCOPY, 1994, 7 (03) :243-254